How Do CMIP6 HighResMIP Models Perform in Simulating Precipitation Extremes over East Africa?
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Published:2024-07-20
Issue:7
Volume:11
Page:106
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ISSN:2306-5338
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Container-title:Hydrology
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language:en
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Short-container-title:Hydrology
Author:
Babaousmail Hassen1, Ayugi Brian Odhiambo2ORCID, Lim Kam Sian Kenny Thiam Choy1ORCID, Randriatsara Herijaona Hani-Roge Hundilida3, Mumo Richard4ORCID
Affiliation:
1. School of Atmospheric Science and Remote Sensing, Wuxi University, Wuxi 214105, China 2. Faculty of Civil Engineering, Seoul National University of Science and Technology, 232 Gongneung-ro, Nowon-gu, Seoul 01811, Republic of Korea 3. Department of Atmospheric Physics, Faculty of Mathematics and Physics, Charles University, 121 16 Prague, Czech Republic 4. Department of Mathematics and Statistical Sciences, Botswana International University of Science and Technology, Private Bag 16, Palapye Plot 10071, Botswana
Abstract
This work assesses the ability of nine Coupled Model Intercomparison Project phase 6 (CMIP6) High-Resolution Model Intercomparison Project (HighResMIP) models and their ensemble mean to reproduce precipitation extremes over East Africa for the period 1995–2014. The model datasets are assessed against two observation datasets: CHIRPS and GPCC. The precipitation indices considered are CDD, CWD, R1mm, R10mm, R20mm, SDII, R95p, PRCPTOT, and Rx1day. The overall results show that HighResMIP models reproduce annual variability fairly well; however, certain consistent biases are found across HighResMIP models, which tend to overestimate CWD and R1mm and underestimate CDD and SDII. The HighResMIP models are ranked using the Taylor diagram and Taylor Skill Score. The results show that the models reasonably simulate indices, such as PRCPTOT, R1mm, R10mm, R95p, and CDD; however, the simulation of SDII CWD, SDII, and R20mm is generally poor. They are CMCC-CM2-VHR4, HadGEM31-MM, HadGEM3-GC31-HM, and GFDL-CM4. Conversely, MPI-ESM1-2-XR and MPI-ESM1-2-HR show remarkable performance in simulating the OND season while underestimating the MAM season. A comparative analysis demonstrates that the MME has better accuracy than the individual models in the simulation of the various indices. The findings of the present study are important to establish the ability of HighResMIP data to reproduce extreme precipitation events over East Africa and, thus, help in decision making. However, caution should be exercised in the interpretation of the findings based on individual CMIP6 models over East Africa given the overall weakness observed in reproducing mean precipitation.
Reference81 articles.
1. Masson-Delmotte, V., Zhai, P., Pirani, A., Connors, S.L., Péan, C., Berger, S., Caud, N., Chen, Y., Goldfarb, L., and Gomis, M.I. (2021). Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press. 2. WMO (2023, February 02). Greater Horn of Africa Faces 5th Failed Rainy Season. Available online: https://public.wmo.int/en/media/news/greater-horn-of-africa-faces-5th-failed-rainy-season. 3. Drought, Local Institutional Contexts, and Support for Violence in Kenya;Linke;J. Confl. Resolut.,2018 4. Droughts in East Africa: Causes, impacts and resilience;Gebremeskel;Earth-Sci. Rev.,2019 5. Climate Extremes: Observations, Modeling, and Impacts;Easterling;Science,2000
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